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赤道X射线发射:对木星高层热层高温的影响。

Equatorial X-ray Emissions: Implications for Jupiter's High Exospheric Temperatures.

作者信息

Waite JH, Gladstone GR, Lewis WS, Drossart P, Cravens TE, Maurellis AN, Mauk BH, Miller S

机构信息

J. H. Waite Jr., G. R. Gladstone, W. S. Lewis, Department of Space Science, Southwest Research Institute, Post Office Box 28510, San Antonio, TX 78228-0510, USA. P. Drossart, DESPA, Observatoire de Paris, F-92195 Meudon Cedex, France. T. E. Cravens and A. N. Maurellis, Department of Physics and Astronomy, University of Kansas, Lawrence, KS 66045-2151, USA. B. H. Mauk, Applied Physics Laboratory, The Johns Hopkins University, Laurel, MD 20723-6099, USA. S. Miller, Department of History, Philosophy, and Communication in Science, University College London, London WC1E 6BT, UK.

出版信息

Science. 1997 Apr 4;276(5309):104-8. doi: 10.1126/science.276.5309.104.

Abstract

Observations with the High Resolution Imager on the Rontgensatellit reveal x-ray emissions from Jupiter's equatorial latitudes. The observed emissions probably result from the precipitation of energetic (>300 kiloelectron volts per atomic mass unit) sulfur and oxygen ions out of Jupiter's inner radiation belt. Model calculations of the energy deposition by such heavy ion precipitation and of the resulting atmospheric heating rates indicate that this energy source can contribute to the high exospheric temperatures(>800 kelvin at 0.01 microbar) measured by the Galileo probe's Atmospheric Structure Instrument. Low-latitude energetic particle precipitation must therefore be considered, in addition to other proposed mechanisms such as gravity waves and soft electron precipitation, as an important source of heat for Jupiter's thermosphere.

摘要

利用伦琴卫星上的高分辨率成像仪进行的观测揭示了木星赤道纬度的X射线辐射。观测到的辐射可能是由于高能(每原子质量单位大于300千电子伏特)的硫离子和氧离子从木星的内辐射带沉降所致。通过这种重离子沉降进行的能量沉积以及由此产生的大气加热率的模型计算表明,这种能量来源有助于伽利略探测器的大气结构仪器所测得的高逸散层温度(在0.01微巴时大于800开尔文)。因此,除了诸如重力波和软电子沉降等其他提出的机制之外,低纬度高能粒子沉降必须被视为木星热层热量的一个重要来源。

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